Relevant bibliographies by topics / Glacial ecosystems

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Glacial ecosystems'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Glacial ecosystems"

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Hodson, Andy, Alexandre M. Anesio, Martyn Tranter, et al. "GLACIAL ECOSYSTEMS." Ecological Monographs 78, no. 1 (2008): 41–67. http://dx.doi.org/10.1890/07-0187.1.

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Nolan, Connor, Jonathan T. Overpeck, Judy R. M. Allen, et al. "Past and future global transformation of terrestrial ecosystems under climate change." Science 361, no. 6405 (2018): 920–23. http://dx.doi.org/10.1126/science.aan5360.

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Impacts of global climate change on terrestrial ecosystems are imperfectly constrained by ecosystem models and direct observations. Pervasive ecosystem transformations occurred in response to warming and associated climatic changes during the last glacial-to-interglacial transition, which was comparable in magnitude to warming projected for the next century under high-emission scenarios. We reviewed 594 published paleoecological records to examine compositional and structural changes in terrestrial vegetation since the last glacial period and to project the magnitudes of ecosystem transformati
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Kennedy, Nick. "Glacial dimples shelter unique ecosystems." New Scientist 225, no. 3013 (2015): 16. http://dx.doi.org/10.1016/s0262-4079(15)60527-9.

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Sharma, Birendra Prasad, Subash Adhikari, Ganesh Paudel, and Namita Paudel Adhikari. "Microbial Diversity in the Glacial Ecosystem of Antarctic, Arctic, and Tibetan Plateau: Properties and Response to the Environmental Condition." Janapriya Journal of Interdisciplinary Studies 9, no. 1 (2020): 231–50. http://dx.doi.org/10.3126/jjis.v9i1.35239.

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Microorganisms, as successive members of the food web, play a major role in biological processes. They are found in environments ranging from extremely hot to harsh cold temperatures. Thus, the study of bacterial communities in various ecosystems is of great concern around the world. The glacier is one of the parts of the cryosphere, which is the key component and sensitive indicator of climatic and environmental changes. A glacial ecosystem is a habitat for various microorganisms, i.e., autotrophic and heterotrophic. Different physicochemical parameters like temperature, pH, electrical conduc
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Gíslason, Gísli Már, Jón S. Ólafsson, and Hákon Adalsteinsson. "Life in Glacial and Alpine Rivers in Central Iceland in Relation to Physical and Chemical Parameters." Hydrology Research 31, no. 4-5 (2000): 411–22. http://dx.doi.org/10.2166/nh.2000.0025.

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The characteristics of stream and river ecosystems in arctic and alpine areas are determined mainly by the relative contribution of glacial meltwater, snowmelt, rainfall and groundwater. Each source generates a particular seasonal hydrological signature, affecting physical and chemical properties, and hence biological communities. The relative contribution of each source is sensitive to climate change. The study was concentrated on the glacial River W-Jökulsá and some non-glacial rivers in the central highlands of Iceland. The water in the glacial river was entirely glacial meltwater at the gl
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Nielsen, Julie K., S. James Taggart, Thomas C. Shirley, and Jennifer Mondragon. "Spatial distribution of juvenile and adult female Tanner crabs (Chionoecetes bairdi) in a glacial fjord ecosystem: implications for recruitment processes." ICES Journal of Marine Science 64, no. 9 (2007): 1772–84. http://dx.doi.org/10.1093/icesjms/fsm158.

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AbstractNielsen, J. K., Taggart, S. J., Shirley, T. C., and Mondragon, J. 2007. Spatial distribution of juvenile and adult female Tanner crabs (Chionoecetes bairdi) in a glacial fjord ecosystem: implications for recruitment processes. – ICES Journal of Marine Science, 64: 1772–1784. A systematic pot survey in Glacier Bay, Alaska, was conducted to characterize the spatial distribution of juvenile and adult female Tanner crabs, and their association with depth and temperature. The information was used to infer important recruitment processes for Tanner crabs in glaciated ecosystems. High-catch a
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Stibal, Marek, James A. Bradley, Arwyn Edwards, et al. "Glacial ecosystems are essential to understanding biodiversity responses to glacier retreat." Nature Ecology & Evolution 4, no. 5 (2020): 686–87. http://dx.doi.org/10.1038/s41559-020-1163-0.

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Wadham, Jemma Louise, Jonathan Hawkings, Jon Telling, et al. "Sources, cycling and export of nitrogen on the Greenland Ice Sheet." Biogeosciences 13, no. 22 (2016): 6339–52. http://dx.doi.org/10.5194/bg-13-6339-2016.

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Abstract. Fjord and continental shelf environments in the polar regions are host to some of the planet's most productive ecosystems and support economically important fisheries. Their productivity, however, is often critically dependent upon nutrient supply from upstream terrestrial environments delivered via river systems. In glacially fed coastal ecosystems, riverine nutrients are largely sourced from melting snow and ice. The largest and most extensive glacially fed coastal ecosystem in the Arctic is that bordering the Greenland Ice Sheet. The future primary productivity of this ecosystem,
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Hobbs, William O., Rolf D. Vinebrooke, and Alexander P. Wolfe. "Biogeochemical responses of two alpine lakes to climate change and atmospheric deposition, Jasper and Banff National parks, Canadian Rocky Mountains." Canadian Journal of Fisheries and Aquatic Sciences 68, no. 8 (2011): 1480–94. http://dx.doi.org/10.1139/f2011-058.

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The sensitivity of remote alpine ecosystems to global change has been documented by 20th century changes in climate, glacial recession, and terrestrial and aquatic ecosystems. Here we present sedimentary records of biogeochemical responses in two alpine lake ecosystems to multiple environmental drivers over the last ∼500 years in Banff and Jasper National Parks (Alberta, Canada). We combine paleoecological measures of primary production and diatom community structure with geochemical proxies of reactive N (Nr) deposition to describe the nature and rate of recent ecosystem changes. Curator Lake
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Mykitchak, T. I. "Transformation of ecosystems glacial lakes in Ukrainian Carpathians." Ecology and Noospherology 28, no. 3-4 (2017): 28–36. http://dx.doi.org/10.15421/031713.

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The sizes of glacial lakes of the Ukrainian Carpathians without surface water runoff (Brebeneskul, Nesamovyte – the last 130 years, Verhne Ozirne, Nyzhne Ozirne – the last 50 years) and surface water runoff lakes Dogyaska (the last 30 years) has not substantial changes. The lakes Maricheyka and Vorozheska considerably decreased in area (20–40 % of previous squares), obviously, due to the erosion of rocky moraines-damages. Comparison of photos lakes Nesamovyte (1935–2008) has not showed changes of the outlines of the water area, the sedge-sphagnum alloy and the coastal thickets of the debris. T
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Dissertations / Theses on the topic "Glacial ecosystems"

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Mueller, Derek. "A bipolar comparison of glacial cryoconite ecosystems /." Thesis, McGill University, 2001. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=33017.

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This thesis compares the habitat and community ecology of cylindrical meltholes from the surface of two polar glaciers. These holes (termed cryoconite holes) are formed when wind-blown dust gathers in small depressions in the ice causing vertical melting by absorption of more radiation than the surrounding ice. The communities are complex microbial consortia of heterotrophic bacteria, cyanobacteria, eukaryotic algae, and protists. Samples were taken from cryoconite holes on Canada Glacier, Taylor Valley, Antarctica (77°37'S, 162°55'E) and on White Glacier, Axel Heiberg Island, Nunavut Territor
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Le, Mezo Priscilla. "Variabilité des écosystèmes marins de l'échelle inter-annuelle au dernier cycle glaciaire-interglaciaire." Thesis, Université Paris-Saclay (ComUE), 2017. http://www.theses.fr/2017SACLV003/document.

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La variabilité du système climatique influence la productivité et la distribution des espèces marines sur toutes les échelles de temps, de la variabilité saisonnière et inter-annuelle aux cycles glaciaires-interglaciaires. Mais ces liens entre climat et écosystèmes marins sont encore largement méconnus, de telle sorte que les prévisions des changements à venir sont difficiles. De plus, parce que les indicateurs paléoclimatiques issus des archives marines sont souvent liés au fonctionnement de l’écosystème, cette méconnaissance limite la fiabilité de la reconstruction de la variabilité climatiq
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Adams, Jonathan M. "The role of terrestrial ecosystems in glacial-to-interglacial changes in the global carbon cycle : an approach based on reconstruction of paleovegetation : l'Influence des écosystèmes terrestres sur les changements du cycle global du carbone, entre les aires glaciaires et interglaciaires : une approche par la reconstruction de la paléovégétation." Aix-Marseille 2, 1995. http://www.theses.fr/1995AIX22054.

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Les changements du taux atmospherique du co#2 sont d'une grande importance pour l'explication des fluctuations climatiques pendant le quaternaire. Le carbone organique dans les ecosystemes continentaux peut jouer un grand role dans la modification et la direction des fluctuations glaciaire-interglaciaires. Une base de donnees paleo-environnementale est utilisee pour construire des cartes de la vegetation des continents, a 18000, 8000 et 5000 ans. Ces cartes permettent de calculer les bilans du carbone pour chaque periode. Les calculs indiquent qu'il y a une augmentation d'environ 1700 gt (+/-
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Khamis, Kieran. "Climate change and glacier retreat in the French Pyrénées : implications for Alpine river ecosystems." Thesis, University of Birmingham, 2014. http://etheses.bham.ac.uk//id/eprint/4927/.

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Climate change disproportionately threatens alpine river ecosystems due to the strong connections between cryosphere, hydrology and physicochemical habitat. Our general understanding of how these systems will respond to warming is, however, based on conceptual models derived from studies undertaken at relatively small spatial scales. This research utilizes: (i) field data collected from five glacierized river basins in the French Pyrénées; (ii) field based experimentation; and (iii) climate/hydrological modelling, to improve understanding of alpine river ecosystem change. Despite a linear, har
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Ding, Yan. "Environmental Dynamics of Dissolved Black Carbon in Aquatic Ecosystems." FIU Digital Commons, 2013. http://digitalcommons.fiu.edu/etd/846.

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Black carbon (BC), the incomplete combustion product from biomass and fossil fuel burning, is ubiquitously found in soils, sediments, ice, water and atmosphere. Because of its polyaromatic molecular characteristic, BC is believed to contribute significantly to the global carbon budget as a slow-cycling, refractory carbon pool. However, the mass balance between global BC generation and accumulation does not match, suggesting a removal mechanism of BC to the active carbon pool, most probable in a dissolved form. The presence of BC in waters as part of the dissolved organic matter (DOM) pool was
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Kern, Jennifer M. "Modelling hydrologic system change in a paraglacial catchment in the Northern Rocky Mountains." Thesis, Virginia Tech, 2021. http://hdl.handle.net/10919/103778.

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The Northern Rocky Mountains, home to the highest concentration of glaciers in the American West, are undergoing increased rates of climate warming, resulting in previously unseen ecological and hydrological outcomes. Globally, many glacier basins have experienced glacial recession to the threshold point of surpassing peak basin runoff, resulting in substantial decreases in local hydrological yield. Such findings call for models that do not alone examine glacial runoff but a complete examination of changes in the water budget. Alpine catchments are increasingly vulnerable to evapotranspirative
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Williams, Thomas James. "Estimating organic carbon on avalanche paths in Glacier National Park, Montana." Thesis, University of Iowa, 2014. https://ir.uiowa.edu/etd/4795.

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Avalanche paths are unique ecosystems that represent a significant portion of the landscape in the northern Rocky Mountains. Frequent avalanche disturbance results in vegetative cover that is unlike the adjacent coniferous forest. These high relief environments have the potential to remove carbon from the atmosphere at rates differing from those of the surrounding forest, and to regulate matter and/or energy fluxes to downslope ecosystems. This thesis attempts to estimate organic carbon on south-facing avalanche paths in the southern portion of Glacier National Park, Montana. I am specifically
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Michaels, Amanda Paige. "Land Use and Land Cover Change in the Crown of the Continent Ecosystem, Montana, USA from 1992-2011." Thesis, Virginia Tech, 2016. http://hdl.handle.net/10919/72842.

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In recent decades land use and land cover change (LULCC) has occurred throughout the Intermountain West. The Crown of the Continent Ecosystem (CCE) extends along the Rocky Mountains adjacent to the Canada-U.S. International border. In the U.S. portion of the CCE, located in northwestern Montana, development has increased since the 1990s, largely because of urban to rural migration. The CCE has become an amenity-based destination, which in turn is likely to threaten its terrestrial and aquatic ecological diversity (Quinn and Broberg 2007). Specifically, development pressures on private lands su
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Reckin, Rachel Jean. "Mountains as crossroads : temporal and spatial patterns of high elevation activity in the Greater Yellowstone ecosystem, USA." Thesis, University of Cambridge, 2018. https://www.repository.cam.ac.uk/handle/1810/278102.

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In the archaeological literature, mountains are often portrayed as the boundaries between inhabited spaces. Yet occupying high elevations may have been an adaptive choice for ancient peoples, as rapidly changing elevations also offer variation in climate and resources over a relatively small area. So what happens, instead, if we put mountain landscapes at the center of our analyses of prehistoric seasonal rounds and ecological adaptation? This Ph.D. argues that, in order to understand any landscape that includes mountains, from the Alps to the Andes, one must include the ecology and archaeolog
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Quenta, Herrera Estefania. "Structure multi-échelles de la biodiversité aquatique d'écosystèmes alpins sous l'influence du changement climatique." Thesis, Tours, 2017. http://www.theses.fr/2017TOUR4015/document.

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En combinant des approches empiriques et expérimentales, nous avons évalué les effets de trois composantes du changement climatique sur la biodiversité aquatique alpine: le recouvrement glaciaire, le gradient altitudinal et la température de l'eau. Nous avons montré que: 1) Les niveaux intermédiaires de recouvrement glaciaire génèrent une hétérogénéité environnementale élevée associée à une plus grande diversité locale du zooplancton. 13% de la diversité régionale est limitée aux tourbières aux bassins fortement englacés, et pourrait être amenée à disparaître avec le réchauffement. 2) Les filt
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Books on the topic "Glacial ecosystems"

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Regan, Claudia M. Vegetation of the Glacier Lakes Ecosystem Experiments Site. Forest Service, Rocky Mountain Research Station, 1998.

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Nowacki, Gregory J. Ecological subsections of southeast Alaska and neighboring areas of Canada. U.S. Dept. of Agriculture, Forest Service, Alaska Region, 2001.

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Service, United States Forest, and British Columbia. Ministry of Environment, Lands, and Parks., eds. Ecological subsections of southeast Alaska and neighboring areas of Canada. U.S. Dept. of Agriculture, Forest Service, Alaska Region, 2001.

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R, Lembersky Mark, ed. Nisqually watershed: Glacier to Delta : a river's legacy. Mountaineers, 1995.

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Vuorinen, Ilppo. Post-Glacial Baltic Sea Ecosystems. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.675.

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Post-glacial aquatic ecosystems in Eurasia and North America, such as the Baltic Sea, evolved in the freshwater, brackish, and marine environments that fringed the melting glaciers. Warming of the climate initiated sea level and land rise and subsequent changes in aquatic ecosystems. Seminal ideas on ancient developing ecosystems were based on findings in Swedish large lakes of species that had arrived there from adjacent glacial freshwater or marine environments and established populations which have survived up to the present day. An ecosystem of the first freshwater stage, the Baltic Ice La
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Microbiology and biogeochemistry of glacial and permafrost environments. International Glaciological Society, 2010.

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Biodiversity and evolution of glacial water ecosystems in the Rila Mountains. Institute of Zoology, Ministry of Environment and Waters, 2000.

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C, Musselman Robert, Connell B. H, and Rocky Mountain Forest and Range Experiment Station (Fort Collins, Colo.), eds. The Glacier Lakes Ecosystem Experiments Site. U.S. Dept. of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station, 1994.

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Naidenov, W. T. Biodiversity and Evolution of Glacier Water Ecosystems in the Rila Mountains. Akademicno Izdatelstvo, 2000.

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The Remembered Land: Surviving Sea-level Rise after the Last Ice Age. Bloomsbury Academic, 2015.

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Book chapters on the topic "Glacial ecosystems"

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Takeuchi, Nozomu. "Glacial Ecosystems." In Encyclopedia of Earth Sciences Series. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_608.

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Milner, Alexander M. "Glacial Recession and Freshwater Ecosystems in Coastal Alaska." In Ecological Studies. Springer New York, 1997. http://dx.doi.org/10.1007/978-1-4612-0677-4_12.

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Puhe, Joachim, and Bernhard Ulrich. "Post-Glacial Development of Climate and Forest Ecosystems." In Ecological Studies. Springer Berlin Heidelberg, 2001. http://dx.doi.org/10.1007/978-3-642-59531-8_3.

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Johnson, Chris E., Robert J. Petras, Richard H. April, and Thomas G. Siccama. "Post-Glacial Lead Dynamics in a Forest Soil." In Biogeochemical Investigations of Terrestrial, Freshwater, and Wetland Ecosystems across the Globe. Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-94-007-0952-2_39.

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Uehlinger, U., C. T. Robinson, M. Hieber, and R. Zah. "The physico-chemical habitat template for periphyton in alpine glacial streams under a changing climate." In Global Change and River Ecosystems—Implications for Structure, Function and Ecosystem Services. Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-94-007-0608-8_8.

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Galkovskaya, Galina A., and Vadim V. Arapov. "Spatial structure and ecological efficiency in the summer zooplankton of a glacial lake." In Eutrophication in Planktonic Ecosystems: Food Web Dynamics and Elemental Cycling. Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-017-1493-8_25.

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Prentice, Michael L., Johan L. Kleman, and Arjen P. Stroeven. "The Composite Glacial Erosional Landscape of the Northern Mcmurdo Dry Valleys: Implications for Antarctic Tertiary Glacial History." In Ecosystem Dynamics in a Polar Desert: the Mcmurdo Dry Valleys, Antarctica. American Geophysical Union, 2013. http://dx.doi.org/10.1029/ar072p0001.

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Kohshima, Shiro, Yoshitaka Yoshimura, and Nozomu Takeuchi. "Glacier Ecosystem and Biological ICE-Core Analysis." In Series of the Centro de Estudios Científicos. Springer US, 2002. http://dx.doi.org/10.1007/978-1-4615-0645-4_1.

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Obolewski, Krystian. "Biodiversity of Macroinvertebrates in Oxbow-Lakes of Early Glacial River Basins in Northern Poland." In Ecosystems Biodiversity. InTech, 2011. http://dx.doi.org/10.5772/23659.

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Smith, Raymond C., and Douglas G. Goodin. "Introductory Overview." In Climate Variability and Ecosystem Response in Long-Term Ecological Research Sites. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195150599.003.0030.

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Elias argues (chapter 18, p. 370) that ecosystems are shaped by environmental changes that have occurred over thousands of years so that the century to millennial timescale is of particular significance because “it is on these timescales that ecosystems form, break apart, and reform in new configurations.” Within this context, the authors for the three chapters in part IV evaluate evidence for climate variability since the Last Glacial Maximum (LGM) to the present. They evaluate the biological responses to these longer term changes and highlight the importance of past climatic conditions on current ecosystem function. If we view, as Elias does, glacial climate as a filter through which ecosystems have passed, then variability since the LGM comprises a significant fraction of the biotic history that shaped current ecosystems. This is an overriding theme for this section. Fountain and Lyons (chapter 16), examining a dry valley ecosystem in Antarctica (MCM), evaluate various proxy records to establish the historic context of their landscape. They argue that this historical context is important for a full understanding of ecosystems and that it is especially important for the MCM ecosystem. Providing an excellent example of legacy, the effect of past imprints on current ecosystem function, they present evidence that past climatic variations truly dictate current ecosystem status. During the LGM, ice blocked the current Taylor Valley, forming a lake that contained phytoplankton and algal mats. Subsequent warming eliminated the blockage, drained the large lake, forming several smaller ones, and established the current landscape. The former large lake supplied nutrients to the soil and current lakes. Fountain and Lyons (p. 334) state that “the vital importance of climatic legacy in the dry valleys is due to its extreme environment, low biodiversity, and short food chains.” They also observe a “polar amplification,” whereby the sharp solid/liquid phase transition of water allows small changes in climate to produce relatively large variations in ecosystem response. The Jornada Long-Term Ecological Research site (JRN) is representative of the desert shrubland and desert grassland ecosystems of the southwestern United States. Monger (chapter 17) makes use of a range of biotic (packrat middens, fossil pollen), abiotic (chronological data on lake levels, position of alpine glaciers and rock glaciers) and soil-geomorphic evidence to create a working hypothesis of the bioclimatic changes during the last 20,000 years. There is a remarkable consistency in these proxy estimates given their diversity.
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Conference papers on the topic "Glacial ecosystems"

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Tilg, Markus, Michael Storrie-Lombardi, Christoph Kohstall, Andreas Trenkwalder, Roland Psenner, and Birgit Sattler. "L.I.F.E.: laser induced fluorescence emission, a non-invasive tool to detect photosynthetic pigments in glacial ecosystems." In SPIE Optical Engineering + Applications, edited by Richard B. Hoover, Paul C. W. Davies, Gilbert V. Levin, and Alexei Y. Rozanov. SPIE, 2011. http://dx.doi.org/10.1117/12.893586.

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Burra, K. G., and A. K. Gupta. "Isothermal Splitting of CO2 to CO Using Cobalt-Ferrite Redox Looping." In ASME 2020 Power Conference collocated with the 2020 International Conference on Nuclear Engineering. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/power2020-16960.

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Abstract Rising atmospheric CO2 levels from significant imbalance between carbon emissions from fossil fuel utilization, especially for energy and chemicals, and natural carbon sequestration rates is known to drive-up the global temperatures and associated catastrophic climate changes, such as rising mean sea level, glacial melting, and extinction of ecosystems. Carbon capture and utilization techniques are necessary for transition from fossil fuel infrastructure to renewable energy resources to help delay the dangers of reaching to the point of positive feedback between carbon emissions and c
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Goff, Paepin. "IDENTIFYING ROCK GLACIER LANDFORMS IN THE GREATER YELLOWSTONE ECOSYSTEM: METHODOLOGY, TAXONOMY, AND A PRIMARY INVENTORY." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-276724.

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De Silva, Shelton G. "Knowledge of Arctic and EQQ Unmanned Aerial Vehicles for Multiple Applications." In ASME 2013 32nd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2013. http://dx.doi.org/10.1115/omae2013-11477.

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The rapid change in climate conditions, and the present demand for political and commercial interest in the Arctic region will cause considerable implications on the environment, ecosystem, security, and on the social system in the region. Today, governments, scientists and researchers understand that there is a huge gap of knowledge in the Arctic region and this must be addressed prior to development of the region, or there will be devastating environmental consequences in the future. Existing studies concluded by various organizations including Lloyd’s of London, US Geological Survey and oth
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Reports on the topic "Glacial ecosystems"

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Wells, Aaron, Tracy Christopherson, Gerald Frost, et al. Ecological land survey and soils inventory for Katmai National Park and Preserve, 2016–2017. National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2287466.

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This study was conducted to inventory, classify, and map soils and vegetation within the ecosystems of Katmai National Park and Preserve (KATM) using an ecological land survey (ELS) approach. The ecosystem classes identified in the ELS effort were mapped across the park, using an archive of Geo-graphic Information System (GIS) and Remote Sensing (RS) datasets pertaining to land cover, topography, surficial geology, and glacial history. The description and mapping of the landform-vegetation-soil relationships identified in the ELS work provides tools to support the design and implementation of
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Musselman, R. C. The Glacier Lakes Ecosystem Experiments Site. U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station, 1994. http://dx.doi.org/10.2737/rm-gtr-249.

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Fox, Douglas G., Anna W. Schoettle, and Frank A. Vertucci. Glacier Lakes Ecosystem Experiment Site: an "Experimental" wilderness. U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station, 1987. http://dx.doi.org/10.2737/rm-gtr-149.

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Regan, Claudia M., Robert C. Musselman, and June D. Haines. Vegetation of the Glacier Lakes Ecosystem Experiments Site. U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, 1997. http://dx.doi.org/10.2737/rmrs-rp-1.

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Demuth, M. N., and M. Ednie. A glacier condition and thresholding rubric for use in assessing protected area / ecosystem functioning. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297892.

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